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Monin–Obukhov (M–O) similarity theory describes non-dimensionalized mean flow and mean temperature in the surface layer under non-neutral conditions.
Based on the scaling arguments of last lecture, Monin and Obukhov (1954) suggested that the vertical variation of mean flow and turbulence characteristics.
Produse de slăbire Ekaterinburg
The Monin and Obukhov similarity theory. (Monin and Obukhov, 1954) and the Dear- dorff (1970) convective scaling theory have together provided conceptual .
An analysis in a plane of the stability parameters ζ = z/L (where z is a height above the ground surface and L is the Obukhov length) and bulk Richardson .